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DOE-STD-3013-2000
A key conclusion from all the work described above is that plutonium container
environments have inherent self-limiting mechanisms that prevent accumulation
of significant pressures of oxygen and hydrogen over calcined oxides. These
mechanisms are very likely to limit buildup of unacceptable pressures of either
hydrogen or oxygen alone. Known mechanisms limiting oxygen buildup include
recombination with hydrogen and formation of PuO2+x from adsorbed water.
Mechanisms that limit hydrogen buildup include recombination with oxygen to
produce water and probably reduction of PuO2+x and other high valent materials
by hydrogen. It is therefore very likely that the bounding gas assumption made
in this Standard (and in DOE-STD-3013-96) is highly conservative.
4) Minimize potential for water readsorption above the 0.5 wt% threshold
MIS measurements on 33 items from Rocky Flats and Hanford which will be
stabilized according to this Standard, show that pure and impure oxide material
2
o
surface areas below 5 m /gram generally result from calcination at 950 C for two
hours. [Haschke/Ricketts 1995; Haschke/Ricketts 1997; Haschke/Martz 1998;
Mason et al. 1999; Manchuron-Mandard/Madic 1996]. This work also shows that
post-calcination water readsorption on oxide particles should not pose a practical
problem with respect to the 0.5 wt% criterion of this Standard (readsorption
onto salt is discussed in the preceding section).
5) Stabilize any other potential gas-producing constituents
This Standard's calcination criterion (2 hrs at 950C) is intended to ensure that in
addition to moisture, all other potential gas-producing impurities in plutonium-
bearing oxide materials are eliminated. The technical literature shows that
nitrates, sulfates and carbonates of plutonium are effectively converted to oxides
by calcination at 950C [Waterbury et al. 1961]. All other nitrates and
carbonates are expected to be decomposed by this procedure. Sulfate is known
to be incorporated into plutonium oxide prepared by peroxide precipitation from
sulfuric acid solutions [Leary et al. 1957]. The report of Moseley and Wing
[Moseley/Wing 1965] shows that 950C calcination is sufficient to destroy this
sulfate constituent. Literature searches indicate that deleterious amounts of
radiolytic gases from residual sulfate and chloride contaminants are unlikely in
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